IsoEnergy and Purepoint Confirm Uranium Discovery In Initial Drilling at the Dorado Joint Venture Project
Highlights
- Initial drillholes at the Q48 target, located in the southern portion of the Project, have intersected uranium mineralization, confirming the zone as a significant uranium-bearing structure. (Figure 2).
- Drillholes PG25-04 and PG25-05 intersected a steeply dipping, north-south trending mineralized structure at vertical depths of 60 and 20 metres below the unconformity, respectively.
- Radioactivity readings from downhole probe measurements averaged 11,050 cps over 3.7 metres with a maximum of 74,800 in PG25-04, and 27,750 over 2.3 metres with a maximum of 79,800 in PG25-05 (See Table 1 for full details).
- Mineralization is hosted within strongly clay-altered basement rocks—considered key indicators of a uranium-bearing hydrothermal system consistent with known Athabasca-style deposits.
- Q48 was originally highlighted as a high-priority target based on historic drilling that encountered structurally disrupted, altered basement rocks with weak radioactivity, and further confirmed in 2022 by IsoEnergy's identification of brittle faults, shearing, and alteration along the conductive trend.
- A third follow-up hole is underway to further track the mineralized structure along the Q48 conductive corridor to the northeast. Approximately 5,400 metres in 18 drill holes are planned for the Project in 2025.
"This is exactly the kind of start we were aiming for. These early results suggest we're on the trail of something meaningful." said
DDHs PG25-04 and PG25-05
Drill hole PG25-04 targeted the Q48 conductor (Figure 1) approximately 800 metres northwest of
Hole PG25-05 was collared using the same azimuth as PG25-04 and intercepted the radioactive structure approximately 40 metres up-dip of that hole. The hole encountered the unconformity at 309 metres, clay altered granitic gneiss and pegmatites to 371 metres, then garnet-rich pelitic gneiss, locally with pyrite and graphite, to the completion depth of 498 metres. The central mineralized structure was hosted in a sheared / brecciated reddish-brown altered granitic gneiss (Figure 4) and returned an average of 75,660 cps over 0.4 metres.
Table 1: Downhole Gamma Results of Drill Holes PG25-04 and PG25-05
Hole ID |
From (m) |
To (m) |
Length (m) |
Avg. cps |
Max. cps |
PG25-04 |
248.7 |
249.4 |
0.7 |
660 |
1,010 |
|
366.0 |
367.0 |
1.0 |
690 |
810 |
|
374.5 |
275.4 |
0.9 |
810 |
1,050 |
|
383.7 |
387.4 |
3.7 |
11,050 |
74,800 |
Includes |
384.7 |
385.1 |
0.4 |
64,220 |
|
PG25-05 |
296.7 |
297.7 |
1.0 |
790 |
960 |
|
325.0 |
327.3 |
2.3 |
27,750 |
79,800 |
Includes |
326.1 |
326.5 |
0.4 |
75,660 |
|
|
328.8 |
329.8 |
1.0 |
730 |
1,000 |
|
395.8 |
396.3 |
0.5 |
1,770 |
2,680 |
Note: Mt. Sopris 2PGA probe used to record downhole gamma readings |
The Q48 zone lies within the southern portion of the Project and is characterized by a steeply dipping, north-south trending conductive package identified through geophysical surveys. Historic drilling in the area intersected strongly altered and structurally disrupted rocks at the unconformity and in the basement, including garnetiferous pelitic gneiss, graphitic pelitic gneiss, and semipelite, with local weak radioactivity and zones of intense clay alteration. These results, combined with the geophysical response, highlighted Q48 as a highly prospective but underexplored target.
Drilling by
About the
Dorado is the flagship project of the IsoEnergy-Purepoint 50/50 joint venture, a partnership encompassing more than 98,000 hectares of prime uranium exploration ground. The Project includes the former
Recent drilling by
The shallow unconformity depths across the Dorado property—typically between 30 and 300 metres—allow for highly efficient drilling and rapid follow-up on results.
Gamma Logging and Geochemical Assaying
A
Core samples are submitted to the
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Additionally, the Company holds a promising VMS project currently optioned to and strategically positioned adjacent to and on trend with Foran Mining Corporation's
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